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On local scales, SHP are driven by root water uptake, vegetation and groundwater dynamics. Soil structure influences SHP such as infiltration, soil water redistribution and root water uptake on small scales. In this Review, we describe SHP across scales and examine their links with soil properties, ecosystem processes and climate. However, land-use changes and extreme events are increasingly impacting these processes. Soil hydrological processes (SHP) support ecosystems, modulate the impact of climate change on terrestrial systems and control feedback mechanisms between water, energy and biogeochemical cycles. Nature Reviews Earth & Environment volume 3, pages 573–587 ( 2022) Cite this article
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